A new Summary for Policymakers on the physical sciences, the first of three parts that make up a report to be released over the next 12 months, will be published in Stockholm on Friday.

It will focus on the science underlying changes in temperature in the atmosphere, the oceans and at the poles.

New estimates will be given for the scale of global warming and its impact on sea levels, glaciers and ice sheets.

Levels of certainty

In its last report in 2007, the IPCC stated that "warming of the climate system is unequivocal" and that "most of the observed increase in global average temperatures since the mid-20th Century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations" - in other words, humans burning fossil fuels.

The onset of the current pause coincides with a spike in upper ocean heat uptake around 2002 (lower graph)

It may have begun when energy trapped by greenhouse gases was buried below the surface of the ocean

However, the continuation of the pause in global surface warming beyond 2004 coincides with a decline in upper ocean heat uptake

Understanding the cause of this decline in upper ocean heat content is crucial for explaining the continuation of the pause in surface warming

In the latest draft summary, seen by the BBC, the level of scientific certainty has increased.

The panel states that it is 95% certain that the "human influence on climate caused more than half the observed increase in global average surface temperatures from 1951-2010."

But since 2007, there has been a growing focus on the fact that global average temperatures haven't gone above the level recorded in 1998.

This slowdown, or hiatus as the IPCC refers to it, has been leapt upon by climate sceptics to argue that the scientific belief that emitting carbon dioxide into the atmosphere increases the temperature of the planet, is wrong.

Scientists have attempted to explain the pause in a number of ways, with many arguing that the Earth has continued to warm but that the heat has gone into oceans.

And this week, when the scientists will go through their summary line by line with officials from 195 governments, the pause is likely to be the focus of heated debate.

Chairman of the IPCC Rajendra Pachauri celebrates the panel's share of the Nobel peace prize in 2007

Prof Arthur Petersen is the chief scientist at the Netherlands Environmental Assessment Agency and part of the Dutch delegation that will review the IPCC report.

"Governments are demanding a clear explanation of what are the possible causes of this factor," he told BBC News.

"I expect that this will be a central piece of the summary."

There are likely to be tough negotiations between the parties throughout the week, with governments having already submitted around 1,800 comments on the draft.

Any changes to the text will need to be approved by the scientists, who will want to make sure that they are consistent with the underlying reports. This could lead to some tense moments.

"I wouldn't say there is a reluctance of the authors to take up such an issue as the pause, but they want to do it in a proper way," said Prof Petersen.

"There will remain a tension between how much you can deliver based on the peer-reviewed science and what the governments would like to have."

Too sensitive

In the draft report, the panel agrees that "the rate of warming over the past 15 years (1998-2012) is smaller than the trend since 1951".

The effect of this slowdown means that the future temperature range predicted by the IPCC will be wider than in 2007, and with a lower starting point.

Many sceptical voices believe this is a recognition that the IPCC modelling process has been too sensitive to carbon dioxide, a claim given some credence by the text of the draft which states that some models have "too strong a response to increasing greenhouse gas forcing".

But Prof Jean-Pascal van Ypersele, who is a vice-chair of the IPCC, rejects this idea.

Action that helps cope with the effects of climate change - for example construction of barriers to protect against rising sea levels, or conversion to crops capable of surviving high temperatures and drought.

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